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tures by using an external supermagnet and reused more than
five times. The correlation between the intrinsic properties of
Fe O nanoparticles and their catalytic performance was also
From Figure 1B and the corresponding fitting analysis
(Table 1), we can confirm that the Fe O /C sample is made of
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4
magnetite (Fe O ). The spectrum can be fitted with two mag-
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4
[
37]
investigated based on a series of characterizations.
netic hyperfine sextets. Statistical analysis of the spectrum
showed that the amount of magnetite in the sample is higher
than 86%. There is a broad absorption in the center of the
spectrum, which points to the presence of fluctuation-broad-
Results and Discussion
3
+
ened spectral components. A doublet corresponding to Fe
Fe O /C was prepared by a modified precipitation method
[34]
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species can be found in the spectrum. The Raman spectra of
Fe O /C and bulk Fe O were also measured (Figure 1C). The
(
Scheme 1). Ethanol and ammonia were employed as solvent
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4
and alkali precipitator, respectively. A kind of mesoporous
À1
peaks at 1358 and 1598 cm can be assigned to the D and G
bands of the carbon support, respectively (Figure S1b). These
two peaks are very broad, showing the amorphous character
2
À1
carbon with 6.5 nm pore size and 1392 m g surface area was
used as the carbon support. This carbon material was prepared
with a modified hard-template route, which was reported by
À1
of the carbon support. The peaks at 513 and 660 cm can be
[
31,32]
our group previously.
A large amount of oxygen-contain-
[37,38]
assigned to the E and A modes of Fe O .
The relatively
g
1g
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4
À1
ing functional groups (total amount is about 3.23 mmolg ,
detected by Boehm titration) was present on the surface of
low peak intensity compared with that of bulk Fe O should be
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4
due to the small particle size of Fe O in Fe O /C. This result
3
4
3
4
À1
the carbon support, including carboxylic (0.92 mmolg ), lac-
further confirms that Fe O4 is the main phase of Fe O /C,
3
3
4
À1
À1 [16]
tonic (0.91 mmolg ), and phenolic groups (1.40 mmolg ).
These functional groups endow the carbon surface with hydro-
philic properties. This facilitated the introduction of iron nitrate
ethanol solution and ammonia aqueous solution into the mes-
opores of the carbon support. In addition, the surface oxygen
functional groups could also serve as strongly active sites for
which is in agreement with the results of the XRD and Mçssba-
uer measurements.
N2 adsorption–desorption isotherms showed that Fe O /C
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4
possesses a type IV isotherm accompanied by a H3 hysteresis
loop in the relative pressure range 0.4–0.9, suggesting that the
resultant catalyst maintains the mesoporous structure of the
carbon support (Figure 1D). The surface area and volume of
3
+
anchoring Fe ions.
2
À1
3
À1
Fe O /C are 459 m g and 0.39 cm g , respectively. The mor-
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4
phology of Fe O /C was investigated with high-resolution
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4
transmission electron microscopy. The TEM image of Fe O /C
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(
Figure 2a) shows that the iron oxide is present as 30 nm
nanoparticles on the carbon support. The HR-TEM image of an
individual nanoparticle shows that the d-spacing of the lattice
fringes is approximately 0.24 nm, which can be ascribed to the
[
39,40]
(
311) plane of the Fe O crystals (Figure 2b).
Three well-re-
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4
solved diffraction rings are detected in the selected-area elec-
tron diffraction (SAED) pattern, which can be indexed as the
(
311), (440), and (511) planes of Fe O4 (Figure 2c). The
3
energy-dispersive X-ray (EDX) image (Figure 2d) confirms the
presence of Fe, O, and C elements in the selected area.
The magnetic properties of Fe O /C was studied by using
3 4
Scheme 1. Schematic illustration of the preparation process of Fe O /C.
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4
a vibrating sample magnetometer (VSM) at room temperature.
The applied magnetic field was varied from À20000 Oe to
20000 Oe (Figure 3). Fe O /C exhibits a superparamagnetic
Figure 1A shows the X-ray diffraction (XRD) pattern of
Fe O /C calcined at 4008C under an Ar flow. As a reference,
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4
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bulk Fe O4 was prepared by precipitating a stoichiometric
character with a negligible hysteresis loop. The remnant mag-
3
3
+
2+
[33,34]
À1
molar ratio of Fe and Fe ions with ammonia.
tively sharp diffraction peaks at 2q values of 30.2, 35.6, 43.3,
3.8, 57.3, and 62.98 can be observed in both Fe O /C and bulk
Six rela-
netization (M ) is very small (0.3 emug ), which means that
r
nearly no magnetization remained on Fe O /C when the exter-
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4
5
nal magnetic field was removed. This property is favorable for
its application as a catalyst, as the magnetization cannot influ-
ence the dispersion of Fe O /C in the reaction system. The sat-
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Fe O , which match well with the diffractions from the (220),
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(
311), (400), (422), (511), and (440) lattice planes of cubic in-
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4
[
35,36]
À1
verse spinel magnetite iron oxide (Fe O , JCPDS 65-3107).
uration magnetization of Fe O /C is 12.4 emug . This relatively
3 4
3
4
No peaks assigned to other phases of iron oxide (a-Fe O , for
high value can be attributed to the pure Fe O crystal phase
3 4
2
3
example) were found in the pattern. For Fe O /C, the broad
present in Fe O /C. Taking advantage of the relatively strong
3 4
3
4
peak centered at 24.58 can be assigned to the diffractions from
superparamagnetic property, Fe O /C can be easily separated
3 4
the (002) graphite planes of the carbon support (Figure S1a in
from reaction solution by using an external magnetic field
(Figure 3, inset).
the Supporting Information). It should be note that g-Fe O3
2
has the same XRD pattern as that of Fe O . To exclude the for-
The catalytic performance of Fe O /C was tested in the selec-
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4
57
mation of any g-Fe O phase in the Fe O /C composite, Fe
tive oxidation of benzyl alcohol with air as the oxidant source
(Figure 4). Fe O /C exhibits 93.6% conversion of benzyl alcohol
2
3
3
4
Mçssbauer measurements were carried out (Figure 1B).
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ChemCatChem 2016, 8, 805 – 811
806
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